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| crystalliteÓ¦¸ÃÊÇÖ¸µÄÊǾ§Ì壬һ°ã°üÀ¨µ¥¾§ºÍ¶à¾§¡£grainÊǾ§Á£µÄÒâ˼£¬¾§Á£¿ÉÒÔСÖÁ΢Ã×¼¶µÄ£¬Ò²¿ÉÒԺܴó¡£Èçµ¥¾§Ìå¾ÍÊÇÖ»ÓÉÒ»¸ö¾§Á£¹¹³ÉµÄ¡£¶à¾§Ò»°ãÓɺܶàµÄ¾§Á£¹¹³ÉµÄ£¬¾§Á£Ö®¼ä½Ð×ö¾§½ç¼´boundary. |
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6Â¥2008-12-22 00:57:50
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7Â¥2008-12-22 03:59:59
gentle8306
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crystalliteºÍgrainͨ³£¿ÉÒÔ»¥Óá£Ö»²»¹ýMetallurgist³£ÓÃgrain´ú±í¾§Á££¬»¹Óбíʾ¾§½ç²»Óá°crystallite boundary"¶øÓá°grain boundary¡±¡£ ÏÂÃæÎª°Ù¿Æ×Öµä½âÊÍ£¬Çë²Î¿¼¡£ Encyclopedia > Crystallite A crystallite is a domain of solid-state matter that has the same structure as a single crystal. The crystallised matter is rarely found as single crystal, except for a few cases (gems, silicon single crystals for the electronic industry, single crystals of a nickel-based superalloy for the military aircraft engines). Most of time, it is polycrystalline, i.e. it is made of plenty of single crystals - the crystallites - that "stick" together. The crystallite size can vary from a few nanometers to several millimeters. Metallurgists often refer to "grains"; thus, the boundary between two crystallites is the grain boundary, the fracture can be an intergranular fracture or a transgranular fracture. But the term "crystallite boundary" does not exist, it is "grain boundary". |
8Â¥2008-12-25 08:02:31














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